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Open AccessJournal ArticleDOI

Reflections on O2 as a Biosignature in Exoplanetary Atmospheres.

Victoria S. Meadows
- 01 Oct 2017 - 
- Vol. 17, Iss: 10, pp 1022-1052
TLDR
Environmental factors for abiotic O2 have been identified and will improve the ability to choose optimal targets and measurements to guard against false positives, and thorough evaluation of potential biosignatures works to increase confidence in life detection.
Abstract
Oxygenic photosynthesis is Earth's dominant metabolism, having evolved to harvest the largest expected energy source at the surface of most terrestrial habitable zone planets. Using CO2 and H2O—molecules that are expected to be abundant and widespread on habitable terrestrial planets—oxygenic photosynthesis is plausible as a significant planetary process with a global impact. Photosynthetic O2 has long been considered particularly robust as a sign of life on a habitable exoplanet, due to the lack of known “false positives”—geological or photochemical processes that could also produce large quantities of stable O2. O2 has other advantages as a biosignature, including its high abundance and uniform distribution throughout the atmospheric column and its distinct, strong absorption in the visible and near-infrared. However, recent modeling work has shown that false positives for abundant oxygen or ozone could be produced by abiotic mechanisms, including photochemistry and atmospheric escape. Environm...

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Journal ArticleDOI

Habitability and Biosignatures of Hycean Worlds

TL;DR: In this article, the authors investigate a new class of habitable exoplanets composed of water-rich interiors with massive oceans underlying H2-rich atmospheres, referred to here as Hycean worlds.
Book ChapterDOI

Exoplanet Terra Incognita

TL;DR: An overview of ideas and techniques to resolve albedo features on exoplanetary surfaces can be found in this paper, where the authors present an overview of methods to resolve the features on the exoplanet surface.
Book ChapterDOI

Astrobiology and Development of Human Civilization

TL;DR: A young science interested in the origin, evolution and the distribution of forms of life in the universe and in particular aims to discover other life forms outside the Earth as mentioned in this paper. But not all the scientific community agrees with such classification and some people like Adam Frank likes to talk about the Astrobiology of the Anthropocene.
Journal ArticleDOI

Observing Isotopologue Bands in Terrestrial Exoplanet Atmospheres with the James Webb Space Telescope---Implications for Identifying Past Atmospheric and Ocean Loss.

TL;DR: In this article, post-ocean-loss O2-and CO2-dominated atmospheres, containing a range of trace gas abundances, were used to infer the history of ocean loss and atmospheric escape for terrestrial planets around M dwarfs.
Journal ArticleDOI

Molecular Regulation and Evolution of Redox Homeostasis in Photosynthetic Machinery

TL;DR: A comprehensive comparative bioinformatic analysis of redox regulation in evolutionary distinct photosynthetic cells is presented, highlighting the importance of plant responses to stress cues and genetic manipulation of disturbed redox status for balanced and enhanced photosynthesis efficiency and plant productivity.
References
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Journal ArticleDOI

Habitable zones around main sequence stars

TL;DR: The results suggest that mid-to-early K stars should be considered along with G stars as optimal candidates in the search for extraterrestrial life.
Journal ArticleDOI

The rise of oxygen in Earth’s early ocean and atmosphere

TL;DR: The initial increase of O2 in the atmosphere, its delayed build-up in the ocean, its increase to near-modern levels in the sea and air two billion years later, and its cause-and-effect relationship with life are among the most compelling stories in Earth’s history.
Journal ArticleDOI

Atmospheric Influence of Earth's Earliest Sulfur Cycle

TL;DR: Mass-independent isotopic signatures in Precambrian rocks indicate that a change occurred in the sulfur cycle between 2090 and 2450 million years ago, implying that atmospheric oxygen partial pressures were low and that the roles of oxidative weathering and of microbial oxidation and reduction of sulfur were minimal.
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